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1.- Clastic provenance of Oligocene-Miocene turbidite sandstones from internal domains of the Betic-Rifian Chain (western Mediterranean, Gibraltar Arc) and palaeogeographic implications inferred from the comparison with the Calabria-Peloritani Arc comparison with the Calabria-Peloritani Arc
Tethys Geological Society; Cairo; EGY; Egypt, 2008
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2.- LE FLYSCH OLIGO-MIOCENE DE BENI IDER (RIF, MAROC); EVIDENCE D'UNE ALIMENTATION A PARTIR DES ROCHES PLUTONIQUES, CORRELATIONS A TRAVERS LA CHAINE BETICO-MAGHREBINE ET IMPLICATIONS PALEOGEOGRAPHIQUES ;THE OLIGO-MIOCENE FLYSCH OF THE BENI IDER UNIT, RIF, MOROCCO; SOURCE INDICATION FROM THE PLUTONIC ROCKS, CORRELATIONS THROUGH THE BETIC-MAGHREBIDES BELT AND PALEOGEOGRAPHIC IMPLICATIONS
INSTITUT SCIENTIFIQUE; RABAT; MAR; MOROCCO, 2003
APPORT DES CONNAISSANCES GEOLOGIQUES AU DEVELOPPEMENT DES REGIONS NORD DU MAROC; LA CHAINE RIFAINE DANS SON CADRE MEDITERRANEEN OCCIDENTAL ;GEOLOGICAL UNDERSTANDING OF THE DEVELOPMENT OF NORTHERN MOROCCO; THE RIF IN A WEST MEDITERRANEAN CONTEXT
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